New information augmenting the picture of local environment of the LGM/LGT in the context of the Middle Danube Region
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00094862%3A_____%2F16%3AN0000027" target="_blank" >RIV/00094862:_____/16:N0000027 - isvavai.cz</a>
Výsledek na webu
<a href="http://journals.sagepub.com/doi/abs/10.1177/0959683616640051?journalCode=hola" target="_blank" >http://journals.sagepub.com/doi/abs/10.1177/0959683616640051?journalCode=hola</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1177/0959683616640051" target="_blank" >10.1177/0959683616640051</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
New information augmenting the picture of local environment of the LGM/LGT in the context of the Middle Danube Region
Popis výsledku v původním jazyce
Records of occupation by humans in the period following shortly after the Last Glacial Maximum (LGM; 21 ± 2 kyr cal. BP) are still very rare in Central Europe, since it is inferred that the extreme climatic conditions caused the decolonisation of previously settled areas. Our study focuses on the reconstruction of environmental conditions in the surroundings of the open-air Palaeolithic site, Brno-Štýřice III, which falls within this period. The research concentrated on the study of malacological, pollen and anthracological samples to reconstruct the climate shortly after the LGM. 14C dating places the chronostratigraphic position of the site more precisely at the end of the LGM, more specifically into Last Glacial Termination (LGT); analysis of chipped stone industry identifies the occupation with the Epigravettian settlement. The site represents a significant example of the recurrent habitation of a microclimatically favourable microregion near a watercourse in order to utilise available sources of livelihood. The results of the pollen, anthracological and malacological analyses documented a more or less treeless character of surrounding landscape.
Název v anglickém jazyce
New information augmenting the picture of local environment of the LGM/LGT in the context of the Middle Danube Region
Popis výsledku anglicky
Records of occupation by humans in the period following shortly after the Last Glacial Maximum (LGM; 21 ± 2 kyr cal. BP) are still very rare in Central Europe, since it is inferred that the extreme climatic conditions caused the decolonisation of previously settled areas. Our study focuses on the reconstruction of environmental conditions in the surroundings of the open-air Palaeolithic site, Brno-Štýřice III, which falls within this period. The research concentrated on the study of malacological, pollen and anthracological samples to reconstruct the climate shortly after the LGM. 14C dating places the chronostratigraphic position of the site more precisely at the end of the LGM, more specifically into Last Glacial Termination (LGT); analysis of chipped stone industry identifies the occupation with the Epigravettian settlement. The site represents a significant example of the recurrent habitation of a microclimatically favourable microregion near a watercourse in order to utilise available sources of livelihood. The results of the pollen, anthracological and malacological analyses documented a more or less treeless character of surrounding landscape.
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
AC - Archeologie, antropologie, etnologie
OECD FORD obor
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Návaznosti výsledku
Projekt
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Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2016
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
The Holocene
ISSN
0959-6836
e-ISSN
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Svazek periodika
26
Číslo periodika v rámci svazku
9
Stát vydavatele periodika
GB - Spojené království Velké Británie a Severního Irska
Počet stran výsledku
10
Strana od-do
1345-1354
Kód UT WoS článku
000381283200001
EID výsledku v databázi Scopus
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